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other elevated bodies, the evidence of its lowest positive pres-
sure is to be sought still higher; i. e., more elevated from the
ground.
The air and the earth are believed to be, as a whole, charged
with different electricities, which are continually tending to re-
combine, and are perpetually doing so, by varied degrees, in the
lower strata of the air, some directly by the dry land, but much
more through good conducting bodies that are upon the surface
of the earth. This is because our globe is magnetic, and charged
with negative electricity (magnetic ?), although constantly unit-
ing with the positive of the air; so that over all the surface of
our earth, for a very few feet deep, the air is found at a near
balance, i. e., neither positive nor negative, and the needle of
the electrometer is here almost constantly at zero.
Now, we see that if each drop of rain, or each flake of snow,
is of the same kind of electricity with which the globules of
the clouds were charged, and of which they had indeed served
to form a part, — the whole even, by their agglomeration, — it
is easy to conceive how there is an electric change brought about
with every fall of rain, hail, or snow, since this is carried
onward with them in their fall. Each drop of rain, and each
flake of snow, is doing a work that not only causes the electrom-
eter and the barometer to fluctuate, but also causes joints, nerves,
and bones to feel and confess their united power. Says De la
Rive, wherever it rains there is a region of country, or sea, that
for the time is charged with positive electricity; that this region
is completely surrounded by a zone on all its border, but entirely
oxitside the rain and storm, that is, charged with the negative
electricity. Suppose there is rain falling at a very great distance
from the place of observation, but which is approaching, and
then soon arrives there under the action of the wind, and then
passes onward and over without ceasing to fall, until all is
passed. In that case, the following is the order in which it
occurs, i. e., as the storm clouds approach and pass away: —
1. When the rain is very distant, the instruments indicate
positive electricity in the air, as they do almost always, and even
this with some considerable degree of tension.